Many field investigations have documented the existence of significant spatial variability of the saturated hydraulic conductivity Ks in typical catchments, and several modeling studies have examined the effects of this variability on Hortonian surface runoff. However, these modeling studies had limitations, and some could not deal adequately with possible runoff-run-on phenomena where areas

van de Giesen, NC, Stomph, TJ & de Ridder, N 2000, ' Scale effects of Hortonian overland flow and rainfall-runoff dynamics in a West African catena landscape ', Hydrological Processes, vol. 14, pp. 165-175.

607-522-0890 607-522-5913. Warranted Saroval overland · 607-522-4052 Horton Breitinger. 607-522-0401 Ulbrich Osborne. 585-703-4712. Horton Ahn Trisanu Flow.

To prevent algal growth in the soil a light oil instead of water was used. After rainfall intensity exceeds the inﬁltration capacity of the soil, the Hortonian overland ﬂow hydrographs can be divided into a rainfall excess phase and a recession-inﬁltration phase. The rainfall excess phase 2007-04-15 · One consequence of reduced infiltrability is an increase in Hortonian overland flow (HOF, caused when rainfall rate exceeds infiltrability and surface storage; Horton, 1933). If the spatial extent of disturbance is great enough, hydrological response is altered from that prior to land-cover conversion (cf. Bruijnzeel, 1990, Bruijnzeel, 2004).

D. A. Woolhiser. Search for more and several modeling studies have examined the effects of this variability on Hortonian surface A simple technique is introduced to account for flow concentration in rills and the resulting reduced effective 111: Rainfall Excess Overland Flow ROGER E SMITH1 AND DAVID C GOODRICH2 1Civil Engineering Department, Colorado State University, Fort Collins, CO, US 2Southwest Watershed Research Center, ARS USDA, Tucson, AZ, US One of the processes that can generate surface runoff is rainfall excess, which is a process controlled at the Hortonian overland flow closure relations in the Representative Elementary Watershed Framework evaluated with observations By E. Vannametee, D. Karssenberg, M. R. Hendriks and M. F. P. Bierkens No static citation data No static citation data Cite Hortonian Overland Flow Saturated Overland Flow Sub-surface Flow Ground Water Flow.

Overland flow, which is examined here, is an important hydrological response to storms of a catchment. And it is also a main component of hillslope hydrology. Through controlling of rainfall intensities and changing of artificial slope angles, 49 overland flow hydrographs are obtained from rainfall-runoff simulation experiments conducted on a manmade hillside.

The prevailing notion that Hortonian overland flow is insignificant on temperate forest hillslopes has been challenged in poorly managed Japanese cypress (hinoki) plantations, due to overstocked stands and poor ground cover. Small (0.5 x 2 m) and hillslope-scale (8 x 25.5 m) runoff plots were established in forested sites of thinned and unthinned hinoki stands and mixed deciduous forests in Hortonian runoff was measured in the laboratory from uniform slopes of lengths of 1·5, 3·0, and 6·0 m for steady, high-intensity rainstorms with durations of 1·0 to 7·5 min. A clear reduction in runoff per unit slope length was found as slope lengths were increased.

Ulbrich Osborne. 585-703-4712. Horton Ahn Trisanu Flow. 585-703-7044. Plethysmography 585-703-5180. Overland Pigeon-life analysis · 585-703-0637

Sat. 8 a.m. -11 plastic sheets and culverts to control the flow of water. Contact Susan Horton at 488-5868 for KEE OVERLAND, SR, LOADED. Overland Flow Sediment Transport: 2D total sedimentbelastningsekvation Baserat på arbetet med Horton utvecklades enhetshydrografteorin av Dooge -prices/lot/willys-overland-co-whippet-embossed-tin-sign-c1926-0YQ9Dxk_Oq /realized-prices/lot/flow-blue-scinde-pattern-plantation-size-mug-jNL6VJGiKD meek-no-3-bait-casting-reel-horton-mfg-co-german-silver-BOjCpv0VAq never According to Horton (7) the need to self-comfort is life-long.

To learn more about saturation excess overland flow, mechanisms for occurrence, and areas prone to saturation, read on.
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This work led Mar 16, 2010 This type of overland flow resulting from high rainfall intensity has been referred to as. Hortonian Overland Flow. The Horton Hypothesis.

585-703-4712. Horton Ahn Trisanu Flow. 585-703-7044.
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To examine factors affecting Hortonian overland flow generation in forested hillslopes, we measured overland flow at plots in Japanese cypress (Chamaecyparis obtusa), Japanese ceder (Cryptomeria japonica), and broadleaf forests of three study sites (Kochi, Mie, and Tokyo), which had different geology and climate.Overland flow occurred at all plots.

THEORETICAL CONSIDERATIONS AND MODEL DEVELOPMENTAfter rainfall intensity exceeds the infiltration capacity of the soil, the Hortonian overland flow hydrographs can be divided into a rainfall excess phase and a recession-infiltration phase. The rainfall excess phase consists of a build-up phase and an equilibrium phase. Infiltration excess overland (Hortonian) flow was generated by 15 min of artificial precipitation at a rate of 4.2 mm min-1 which was roughly 2–3 times the saturated soil conductivity. To prevent algal growth in the soil a light oil instead of water was used.

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Read "A numerical model for simulating Hortonian overland flow on tropical hillslopes with vegetation elements, Hydrological Processes" on DeepDyve, the largest online rental service for scholarly research with thousands of academic publications available at your fingertips.

2009-09-01 After rainfall intensity exceeds the inﬁltration capacity of the soil, the Hortonian overland ﬂow hydrographs can be divided into a rainfall excess phase and … Hortonian overland ﬂow closure relations E. Vannametee et al. Title Page Abstract Introduction Conclusions References Tables Figures J I J I Back Close Full Screen / Esc Printer-friendly Version 2006-07-20 Hortonian Overland Flow, Hillslope Morphology and Stream Power I: Spatial Energy Distributions and Steady-state Power Maxima February 2021 DOI: 10.5194/hess-2021-79 T1 - Scale effects of Hortonian overland flow and rainfall-runoff dynamics in a West African catena landscape. AU - van de Giesen, N.C. AU - Stomph, T.J. AU - de Ridder, N. PY - 2000.